Geophysics ◽  
2000 ◽  
Vol 65 (2) ◽  
pp. 502-511 ◽  
Author(s):  
Haoping Huang ◽  
Douglas C. Fraser

The apparent resistivity technique using half‐space models has been employed in helicopter‐borne resistivity mapping for twenty years. These resistivity algorithms yield the apparent resistivity from the measured in‐phase and quadrature response arising from the flow of electrical conduction currents for a given frequency. However, these algorithms, which assume free‐space magnetic permeability, do not yield a reliable value for the apparent resistivity in highly magnetic areas. This is because magnetic polarization also occurs, which modifies the electromagnetic (EM) response, causing the computed resistivity to be erroneously high. Conversely, the susceptibility of a magnetic half‐space can be computed from the measured EM response, assuming an absence of conduction currents. However, the presence of conduction currents will cause the computed susceptibility to be erroneously low. New methods for computing the apparent resistivity and apparent magnetic permeability have been developed for the magnetic conductive half‐space. The in‐phase and quadrature responses at the lowest frequency are first used to estimate the apparent magnetic permeability. The lowest frequency should be used to calculate the permeability because this minimizes the contribution to the measured signal from conduction currents. Knowing the apparent magnetic permeability then allows the apparent resistivity to be computed for all frequencies. The resistivity can be computed using different methods. Because the EM response of magnetic permeability is much greater for the in‐phase component than for the quadrature component, it may be better in highly magnetic environments to derive the resistivity using the quadrature component at two frequencies (the quad‐quad algorithm) rather than using the in‐phase and quadrature response at a single frequency (the in‐phase‐quad algorithm). However, the in‐phase‐quad algorithm has the advantage of dynamic range, and it gives credible resistivity results when the apparent permeability has been obtained correctly.


Geophysics ◽  
2014 ◽  
Vol 79 (6) ◽  
pp. E329-E339 ◽  
Author(s):  
Denys Grombacher ◽  
Jan O. Walbrecker ◽  
Rosemary Knight

Surface nuclear magnetic resonance (NMR) is a geophysical technique that provides the ability to noninvasively image water content in the subsurface. To improve the ability of this method to produce images representative of the true subsurface structure, we require high spatial resolution. We derive a method to provide improved spatial resolution through the use of novel excitation strategies designed to enhance and exploit the information content within the quadrature component of the NMR signal. In a traditional surface NMR experiment, the frequency of the perturbing magnetic field ([Formula: see text]) is chosen to equal the Larmor frequency of the hydrogen nuclei in the subsurface. In this case, it is assumed that the signal phase is determined entirely by the conductivity structure of the subsurface. Several studies have found that modeling the signal phase accurately and inverting a complex-valued NMR signal, can improve the spatial resolution of the surface NMR water content images. We propose alternative excitation schemes designed to generate a complex-valued signal, where the quadrature component can be controlled experimentally and was larger than that generated by the conductivity effects. This allowed a single excitation to provide two samplings of the subsurface properties, one stored in the real component and another in the quadrature component. To test if the alternative sampling strategies can provide improved spatial resolution in surface NMR, we evaluated a synthetic study contrasting the performance of three techniques. We contrasted two techniques designed to generate a complex-valued NMR signal during excitation, called off-resonance excitation and composite pulse excitation, to a traditional on-resonance excitation. We demonstrated that our proposed excitation schemes were able to better resolve boundaries between layers with contrasting properties, and we produced images with improved spatial resolution.


2013 ◽  
Vol 475-476 ◽  
pp. 1629-1632
Author(s):  
Liang Li ◽  
Zong Tao Chi ◽  
Yun Jing Wang ◽  
Zheng Wei Qu

This paper presents a digital compensation device based on two multiplying digital-to-analog converters (M-DAC) whose reference voltages are the same standard AC signals. The output of two M-DACs, which is controlled by software coding, are used as the in-phase and the quadrature component through a reverse proportional amplifier and a derivation circuit respectively. Then the four-quadrant compensative signal can be got after the in-phase and quadrature components have been synthesized. The resolution of digital compensation device is determined by the M-DAC, and usually can be reached to 10ppm of the reference voltage. Measurement results show that the linearity of the presented digital compensation device is about 3.7×10-5.


1999 ◽  
Vol 13 (17) ◽  
pp. 2299-2312 ◽  
Author(s):  
A.-S. F. OBADA ◽  
G. M. ABD AL-KADER

The s-parameterized charactristic function for the superposition of squeezed coherent states (SCS's) is given. The s-parameterized distribution functions for the superposition of SCS's are investigated. Various moments are calculated by using this charactristic function. The Glauber second-order coherence function is calculated. The photon number distribution of the superposition of SCS's studied. Analytical and numerical results for the quadrature component distributions for the superposition of a pair of SCS's are presented. The phase distribution calculated from the integration of s-parameterized distribution function over the phase space. A generation scheme is discussed.


1997 ◽  
Vol 64 (2) ◽  
pp. 167-171 ◽  
Author(s):  
A.B. Matsko ◽  
S.P. Vyatchanin
Keyword(s):  

1993 ◽  
Vol 07 (15) ◽  
pp. 2795-2812
Author(s):  
A.A. BAKASOV

Wave functions have been determined which realize constant squeezing (steady-squeezing states) for a quadrature component of the oscillator with a quadratic self-coupling at an á priori given initial complex amplitude of the oscillator. The set of these wave functions forms a kernel of a special generating operator and is divided into two mutually orthogonal subsets: the subset of superpositions of the states with an even number of quanta of fluctuations around the classical value of the oscillator energy and the subset of analogous states but with odd number of such quanta. The value of the steady squeezing is not a monotonic function of the self-coupling constant and possesses an unexpected minimum. Steady-squeezing states do not minimize the uncertainty product and are not the Gaussian states at the same time.


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